43 results on '"Bauduin S"'
Search Results
2. Cortical thickness abnormalities in long-term remitted Cushing’s disease
- Author
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Bauduin, S. E. E. C., van der Pal, Z., Pereira, A. M., Meijer, O. C., Giltay, E. J., van der Wee, N. J. A., and van der Werff, S. J. A.
- Published
- 2020
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3. Long-term effects of Cushing’s Disease on visuospatial planning and executive functioning
- Author
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Bauduin, S., primary, Van Haalen, F., additional, Giltay, E., additional, Meijer, O., additional, Pereira, A., additional, Van Der Wee, N., additional, and Van Der Werff, S., additional
- Published
- 2022
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4. Genetic underpinnings of sociability in the general population
- Author
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Bralten, J.B., Roth Mota, N., Klemann, C.J.H.M., Witte, Ward De, Laing, E., Collier, D.A., Kluiver, H. de, Bauduin, S., Arango, C., Ayuso-Mateos, J.L., Fabbri, C., Kas, M.J., Wee, N. van der, Penninx, B., Serretti, A., Franke, B., Poelmans, G.J.V., Bralten, J.B., Roth Mota, N., Klemann, C.J.H.M., Witte, Ward De, Laing, E., Collier, D.A., Kluiver, H. de, Bauduin, S., Arango, C., Ayuso-Mateos, J.L., Fabbri, C., Kas, M.J., Wee, N. van der, Penninx, B., Serretti, A., Franke, B., and Poelmans, G.J.V.
- Abstract
Item does not contain fulltext, Levels of sociability are continuously distributed in the general population, and decreased sociability represents an early manifestation of several brain disorders. Here, we investigated the genetic underpinnings of sociability in the population. We performed a genome-wide association study (GWAS) of a sociability score based on four social functioning-related self-report questions from 342,461 adults in the UK Biobank. Subsequently we performed gene-wide and functional follow-up analyses. Robustness analyses were performed in the form of GWAS split-half validation analyses, as well as analyses excluding neuropsychiatric cases. Using genetic correlation analyses as well as polygenic risk score analyses we investigated genetic links of our sociability score to brain disorders and social behavior outcomes. Individuals with autism spectrum disorders, bipolar disorder, depression, and schizophrenia had a lower sociability score. The score was significantly heritable (SNP h(2) of 6%). We identified 18 independent loci and 56 gene-wide significant genes, including genes like ARNTL, DRD2, and ELAVL2. Many associated variants are thought to have deleterious effects on gene products and our results were robust. The sociability score showed negative genetic correlations with autism spectrum, disorders, depression, schizophrenia, and two sociability-related traits-loneliness and social anxiety-but not with bipolar disorder or Alzheimer's disease. Polygenic risk scores of our sociability GWAS were associated with social behavior outcomes within individuals with bipolar disorder and with major depressive disorder. Variation in population sociability scores has a genetic component, which is relevant to several psychiatric disorders. Our findings provide clues towards biological pathways underlying sociability.
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- 2021
5. Salivary markers of stress system activation and social withdrawal in humans
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Bauduin, S., primary, Giltay, E., additional, Noorden, M. Van, additional, Van Der Werff, S., additional, Leeuw, M., additional, Hemert, A. Van, additional, and Van Der Wee, N., additional
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- 2021
- Full Text
- View/download PDF
6. Cortical thickness abnormalities in long-term remitted cushing’s disease
- Author
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Bauduin, S., primary, Van Der Pal, Z., additional, Pereira, A., additional, Meijer, O., additional, Giltay, E., additional, Van Der Wee, N., additional, and Van Der Werff, S., additional
- Published
- 2021
- Full Text
- View/download PDF
7. Water Vapor Vertical Profiles on Mars in Dust Storms Observed by TGO/NOMAD
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Aoki, Shohei, Vandaele, Ann Carine, Daerden, Frank, Villanueva, Geronimo L., Liuzzi, Giuliano, Thomas, Ian R., Erwin, Justin T., Trompet, L., Robert, S., Neary, L., Viscardy, S., Ristic, Bojan, Patel, Manish R., Bellucci, Giancarlo, Bauduin, S., López-Moreno, José Juan, Alonso-Rodrigo, G., Fussen, D., Bolsée, D., Carrozzo, G., Clancy, R. Todd, Cloutis, E., Crismani, M., Da Pieve, F., D'Aversa, E., Kaminski, J., Depiesse, C., Garcia-Comas, M., Etiope, G., Fedorova, A.A., Funke, Bernd, Geminale, A., Gérard, Jean-Claude, Giuranna, M., Karatekin, O., Gkouvelis, L., González-Galindo, F., Holmes, J., Hubert, B., Mumma, M.J., Ignatiev, N.I., Kasaba, Y., Kass, D., Kleinböhl, A., Lanciano, O., Lefèvre, F., Lewis, S., López-Puertas, M., Schneider, Nicholas, Nakagawa, H., Hidalgo López, Ana, Mahieux, A., Mason, J., Mege, D., Neefs, E., Novak, R.E., Oliva, F., Sindoni, G., Piccialli, A., Renotte, E., Ritter, B., Willame, Y., Schmidt, F., Smith, M.D., Teanby, N.A., Thiemann, E., Trokhimovskiy, A., Auwera, J.V., Wolff, M.J., Clairquin, R., Whiteway, J., Wilquet, V., Wolkenberg, P., Yelle, R., del Moral Beatriz, A., Barzin, P., Beeckman, B., Cubas, J., BenMoussa, A., Berkenbosch, S., Orban, A., Biondi, D., Bonnewijn, S., Candini, G.P., Giordanengo, B., Gissot, S., Gomez, A., Hathi, B., Zafra, J.J., Leese, M., Maes, J., Pastor-Morales, M., Mazy, E., Mazzoli, A., Meseguer, J., Morales, R., Perez-grande, I., Queirolo, C., Ristic, R., Gomez, J.R., Saggin, B., Samain, V., Sanz Andres, A., Altieri, F., Sanz, R., Simar, J.-F., Thibert, T., the NOMAD team, López-Valverde, M. A., Hill, Brittany, Belgian Science Policy Office, European Space Agency, Ministerio de Ciencia e Innovación (España), European Commission, UK Space Agency, Agenzia Spaziale Italiana, Ministerio de Ciencia, Innovación y Universidades (España), Fonds de la Recherche Scientifique (Fédération Wallonie-Bruxelles), National Aeronautics and Space Administration (US), and Canadian Space Agency
- Subjects
010504 meteorology & atmospheric sciences ,Storm ,Atmosphere of Mars ,Mars Exploration Program ,Atmospheric sciences ,01 natural sciences ,Trace gas ,Atmosphere ,Geophysics ,Space and Planetary Science ,Geochemistry and Petrology ,Dust storm ,Earth and Planetary Sciences (miscellaneous) ,Environmental science ,Hadley cell ,Water vapor ,0105 earth and related environmental sciences - Abstract
It has been suggested that dust storms efficiently transport water vapor from the near-surface to the middle atmosphere on Mars. Knowledge of the water vapor vertical profile during dust storms is important to understand water escape. During Martian Year 34, two dust storms occurred on Mars: a global dust storm (June to mid-September 2018) and a regional storm (January 2019). Here we present water vapor vertical profiles in the periods of the two dust storms (Ls = 162–260° and Ls = 298–345°) from the solar occultation measurements by Nadir and Occultation for Mars Discovery (NOMAD) onboard ExoMars Trace Gas Orbiter (TGO). We show a significant increase of water vapor abundance in the middle atmosphere (40–100 km) during the global dust storm. The water enhancement rapidly occurs following the onset of the storm (Ls~190°) and has a peak at the most active period (Ls~200°). Water vapor reaches very high altitudes (up to 100 km) with a volume mixing ratio of ~50 ppm. The water vapor abundance in the middle atmosphere shows high values consistently at 60°S-60°N at the growth phase of the dust storm (Ls = 195°–220°), and peaks at latitudes greater than 60°S at the decay phase (Ls = 220°–260°). This is explained by the seasonal change of meridional circulation: from equinoctial Hadley circulation (two cells) to the solstitial one (a single pole-to-pole cell). We also find a conspicuous increase of water vapor density in the middle atmosphere at the period of the regional dust storm (Ls = 322–327°), in particular at latitudes greater than 60°S. ©2019. American Geophysical Union. All Rights Reserved., S. A. is >Charge de Recherches> of the F.R.S.-FNRS. ExoMars is a space mission of the European Space Agency and Roscosmos. The NOMAD experiment is led by the Royal Belgian Institute for Space Aeronomy (IASBBIRA), assisted by Co-PI teams from Spain (IAA-CSIC), Italy (INAF-IAPS), and the United Kingdom (Open University). This project acknowledges funding by the Belgian Science Policy Office, with the financial and contractual coordination by the European Space Agency Prodex Office (PEA 4000103401 and 4000121493), by the Spanish MICINN through its Plan Nacional and by European funds under grants PGC2018-101836-B-I00 and ESP2017-87143-R (MINECO/FEDER), as well as by UK Space Agency through grants ST/R005761/1, ST/P001262/1, ST/R001405/1, and ST/S00145X/1 and Italian Space Agency through grant 2018-2-HH.0. The IAA/CSIC team acknowledges financial support from the State Agency for Research of the Spanish MCIU through the >Center of Excellence Severo Ochoa> award for the Instituto de Astrofisica de Andalucia (SEV-2017-0709). This work was supported by the Belgian Fonds de la Recherche Scientifique-FNRS under grant numbers 30442502 (ET_HOME) and T.0171.16 (CRAMIC) and Belgian Science Policy Office BrainBe SCOOP Project. U.S. investigators were supported by the National Aeronautics and Space Administration. Canadian investigators were supported by the Canadian Space Agency. The results retrieved from the NOMAD measurements used in this article are available on the BIRA-IASB data repository: http://repository.aeronomie.be/?doi= 10.18758/71021054 (Aoki et al., 2019).
- Published
- 2019
8. Water Vapor Vertical Profiles on Mars in Dust Storms Observed by TGO/NOMAD
- Author
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Belgian Science Policy Office, European Space Agency, Ministerio de Ciencia e Innovación (España), European Commission, UK Space Agency, Agenzia Spaziale Italiana, Ministerio de Ciencia, Innovación y Universidades (España), Fonds de la Recherche Scientifique (Fédération Wallonie-Bruxelles), National Aeronautics and Space Administration (US), Canadian Space Agency, Aoki, Shohei, Vandaele, Ann Carine, Daerden, Frank, Villanueva, Geronimo L., Liuzzi, Giuliano, Thomas, Ian R., Erwin, Justin T., Trompet, L., Robert, S., Neary, L., Viscardy, S., Hathi, B., Zafra, J.J., Leese, M., Maes, J., Pastor-Morales, M., Mazy, E., Mazzoli, A., Meseguer, J., Morales, Rafael, Pérez Grande, Isabel, Ristic, Bojan, Queirolo, C., Ristic, R., Gomez, J.R., Saggin, B., Smith, M.D., Samain, V., Sanz Andres, A., Altieri, F., Sanz, R., Simar, J.-F., Patel, Manish R., Thibert, T., the NOMAD team, López-Valverde, M. A., Hill, Brittany, Bellucci, Giancarlo, Bauduin, S., López-Moreno, José Juan, Alonso-Rodrigo, G., Fussen, D., Bolsée, D., Carrozzo, G., Clancy, R. Todd, Cloutis, E., Crismani, M., Da Pieve, F., D'Aversa, E., Kaminski, J., Depiesse, C., Garcia-Comas, M., Etiope, G., Fedorova, A.A., Funke, Bernd, Geminale, A., Gérard, Jean-Claude, Giuranna, M., Karatekin, O., Gkouvelis, L., González-Galindo, F., Holmes, J., Hubert, B., Mumma, M.J., Ignatiev, N.I., Kasaba, Y., Kass, D., Kleinböhl, A., Lanciano, O., Lefèvre, F., Lewis, S., López-Puertas, M., Schneider, Nicholas, Nakagawa, H., Hidalgo López, Ana, Mahieux, A., Mason, J., Mege, D., Neefs, E., Novak, R.E., Oliva, F., Sindoni, G., Piccialli, A., Renotte, E., Ritter, B., Willame, Y., Schmidt, F., Teanby, N.A., Thiemann, E., Trokhimovskiy, A., Auwera, J.V., Wolff, M.J., Clairquin, R., Whiteway, J., Wilquet, V., Wolkenberg, P., Yelle, R., del Moral Beatriz, A., Barzin, P., Beeckman, B., Cubas, J., BenMoussa, A., Berkenbosch, S., Orban, A., Biondi, D., Bonnewijn, S., Candini, G.P., Giordanengo, B., Gissot, Samuel, Gomez, A., Belgian Science Policy Office, European Space Agency, Ministerio de Ciencia e Innovación (España), European Commission, UK Space Agency, Agenzia Spaziale Italiana, Ministerio de Ciencia, Innovación y Universidades (España), Fonds de la Recherche Scientifique (Fédération Wallonie-Bruxelles), National Aeronautics and Space Administration (US), Canadian Space Agency, Aoki, Shohei, Vandaele, Ann Carine, Daerden, Frank, Villanueva, Geronimo L., Liuzzi, Giuliano, Thomas, Ian R., Erwin, Justin T., Trompet, L., Robert, S., Neary, L., Viscardy, S., Hathi, B., Zafra, J.J., Leese, M., Maes, J., Pastor-Morales, M., Mazy, E., Mazzoli, A., Meseguer, J., Morales, Rafael, Pérez Grande, Isabel, Ristic, Bojan, Queirolo, C., Ristic, R., Gomez, J.R., Saggin, B., Smith, M.D., Samain, V., Sanz Andres, A., Altieri, F., Sanz, R., Simar, J.-F., Patel, Manish R., Thibert, T., the NOMAD team, López-Valverde, M. A., Hill, Brittany, Bellucci, Giancarlo, Bauduin, S., López-Moreno, José Juan, Alonso-Rodrigo, G., Fussen, D., Bolsée, D., Carrozzo, G., Clancy, R. Todd, Cloutis, E., Crismani, M., Da Pieve, F., D'Aversa, E., Kaminski, J., Depiesse, C., Garcia-Comas, M., Etiope, G., Fedorova, A.A., Funke, Bernd, Geminale, A., Gérard, Jean-Claude, Giuranna, M., Karatekin, O., Gkouvelis, L., González-Galindo, F., Holmes, J., Hubert, B., Mumma, M.J., Ignatiev, N.I., Kasaba, Y., Kass, D., Kleinböhl, A., Lanciano, O., Lefèvre, F., Lewis, S., López-Puertas, M., Schneider, Nicholas, Nakagawa, H., Hidalgo López, Ana, Mahieux, A., Mason, J., Mege, D., Neefs, E., Novak, R.E., Oliva, F., Sindoni, G., Piccialli, A., Renotte, E., Ritter, B., Willame, Y., Schmidt, F., Teanby, N.A., Thiemann, E., Trokhimovskiy, A., Auwera, J.V., Wolff, M.J., Clairquin, R., Whiteway, J., Wilquet, V., Wolkenberg, P., Yelle, R., del Moral Beatriz, A., Barzin, P., Beeckman, B., Cubas, J., BenMoussa, A., Berkenbosch, S., Orban, A., Biondi, D., Bonnewijn, S., Candini, G.P., Giordanengo, B., Gissot, Samuel, and Gomez, A.
- Abstract
It has been suggested that dust storms efficiently transport water vapor from the near-surface to the middle atmosphere on Mars. Knowledge of the water vapor vertical profile during dust storms is important to understand water escape. During Martian Year 34, two dust storms occurred on Mars: a global dust storm (June to mid-September 2018) and a regional storm (January 2019). Here we present water vapor vertical profiles in the periods of the two dust storms (Ls = 162–260° and Ls = 298–345°) from the solar occultation measurements by Nadir and Occultation for Mars Discovery (NOMAD) onboard ExoMars Trace Gas Orbiter (TGO). We show a significant increase of water vapor abundance in the middle atmosphere (40–100 km) during the global dust storm. The water enhancement rapidly occurs following the onset of the storm (Ls~190°) and has a peak at the most active period (Ls~200°). Water vapor reaches very high altitudes (up to 100 km) with a volume mixing ratio of ~50 ppm. The water vapor abundance in the middle atmosphere shows high values consistently at 60°S-60°N at the growth phase of the dust storm (Ls = 195°–220°), and peaks at latitudes greater than 60°S at the decay phase (Ls = 220°–260°). This is explained by the seasonal change of meridional circulation: from equinoctial Hadley circulation (two cells) to the solstitial one (a single pole-to-pole cell). We also find a conspicuous increase of water vapor density in the middle atmosphere at the period of the regional dust storm (Ls = 322–327°), in particular at latitudes greater than 60°S. ©2019. American Geophysical Union. All Rights Reserved.
- Published
- 2019
9. No detection of methane on Mars from early ExoMars Trace Gas Orbiter observations
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Belgian Science Policy Office, Ministerio de Ciencia e Innovación (España), European Commission, UK Space Agency, Centre National de la Recherche Scientifique (France), Fonds de la Recherche Scientifique (Fédération Wallonie-Bruxelles), Roscosmos, Russian Government, Agenzia Spaziale Italiana, European Space Agency, Korablev, O., Vandaele, Ann Carine, Montmessin, Franck, Fedorova, A. A., Trokhimovskiy, A., Forget, François, Lefèvre, F., Daerden, Frank, Thomas, Ian R., Trompet, L., Erwin, Justin T., Aoki, Shohei, Robert, S., Neary, L., Viscardy, S., Grigoriev, A.V., Ignatiev, N. I., Shakun, Alexey, Patrakeev, A., Belyaev, D.A., Bertaux, J.L., Olsen, K. S., Baggio, L., Alday, J., Ivanov, Y. S., Ristic, Bojan, Mason, J., Willame, Y., Depiesse, C., Hetey, L., Berkenbosch, S., Clairquin, R., Queirolo, C., Beeckman, B., Neefs, E., Patel, Manish R., Bellucci, Giancarlo, López-Moreno, José Juan, Wilson, C. F., Etiope, G., Zelenyi, Lev, Svedhem, H., Vago, J. L., Alonso-Rodrigo, G., Altieri, F., Anufreychik, K., Arnold, G., Bauduin, S., Bolsée, D., Funke, Bernd, García Comas, Maia, González-Galindo, F., López-Puertas, Manuel, López-Valverde, M. A., Martín-Torres, F. J., Vazquez, L., Zorzano, María Paz, Belgian Science Policy Office, Ministerio de Ciencia e Innovación (España), European Commission, UK Space Agency, Centre National de la Recherche Scientifique (France), Fonds de la Recherche Scientifique (Fédération Wallonie-Bruxelles), Roscosmos, Russian Government, Agenzia Spaziale Italiana, European Space Agency, Korablev, O., Vandaele, Ann Carine, Montmessin, Franck, Fedorova, A. A., Trokhimovskiy, A., Forget, François, Lefèvre, F., Daerden, Frank, Thomas, Ian R., Trompet, L., Erwin, Justin T., Aoki, Shohei, Robert, S., Neary, L., Viscardy, S., Grigoriev, A.V., Ignatiev, N. I., Shakun, Alexey, Patrakeev, A., Belyaev, D.A., Bertaux, J.L., Olsen, K. S., Baggio, L., Alday, J., Ivanov, Y. S., Ristic, Bojan, Mason, J., Willame, Y., Depiesse, C., Hetey, L., Berkenbosch, S., Clairquin, R., Queirolo, C., Beeckman, B., Neefs, E., Patel, Manish R., Bellucci, Giancarlo, López-Moreno, José Juan, Wilson, C. F., Etiope, G., Zelenyi, Lev, Svedhem, H., Vago, J. L., Alonso-Rodrigo, G., Altieri, F., Anufreychik, K., Arnold, G., Bauduin, S., Bolsée, D., Funke, Bernd, García Comas, Maia, González-Galindo, F., López-Puertas, Manuel, López-Valverde, M. A., Martín-Torres, F. J., Vazquez, L., and Zorzano, María Paz
- Abstract
The detection of methane on Mars has been interpreted as indicating that geochemical or biotic activities could persist on Mars today1. A number of different measurements of methane show evidence of transient, locally elevated methane concentrations and seasonal variations in background methane concentrations2–5. These measurements, however, are difficult to reconcile with our current understanding of the chemistry and physics of the Martian atmosphere6,7, which—given methane’s lifetime of several centuries—predicts an even, well mixed distribution of methane1,6,8. Here we report highly sensitive measurements of the atmosphere of Mars in an attempt to detect methane, using the ACS and NOMAD instruments onboard the ESA-Roscosmos ExoMars Trace Gas Orbiter from April to August 2018. We did not detect any methane over a range of latitudes in both hemispheres, obtaining an upper limit for methane of about 0.05 parts per billion by volume, which is 10 to 100 times lower than previously reported positive detections2,4. We suggest that reconciliation between the present findings and the background methane concentrations found in the Gale crater4 would require an unknown process that can rapidly remove or sequester methane from the lower atmosphere before it spreads globally. © 2019, The Author(s), under exclusive licence to Springer Nature Limited.
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- 2019
10. A user-friendly computer platform to assess the impact of transport infrastructures on wildlife: A case study with the Eurasian lynx in France
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Bauduin, S., Blanc, Laetitia, Bernard, Cyril, Charbonnel, Anaïs, Chrétien, L., Duchamp, Christophe, Germain, Estelle, Arzhela Hemery, Kramer-Schadt, Stephanie, Marboutin, Eric, Morand, Alain, Zimmermann, Fridolin, and Gimenez, Olivier
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- 2018
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11. Guiding decision-making to mitigate lynx-vehicle collisions using spatially-explicit individual-based models
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Bauduin, S., Blanc, Laetitia, Bernard, Cyril, Charbonnel, Anaïs, Chrétien, L., Duchamp, Christophe, Germain, Estelle, Arzhela Hemery, Kramer-Schadt, Stephanie, Marboutin, Eric, Morand, Alain, Zimmermann, Fridolin, and Gimenez, Olivier
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- 2018
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12. IASI satellite observation of pollutants over China during 10 years
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Clerbaux, Cathy, Boynard, Anne, George, Maya, Hadji-Lazaro, Juliette, Bauduin, S., Clarisse, L., Coheur, Pierre-François, Hurtmans, D., van Damme, M., Wespes, C., Whitburn, S., TROPO - LATMOS, Laboratoire Atmosphères, Milieux, Observations Spatiales (LATMOS), Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Université Pierre et Marie Curie - Paris 6 (UPMC)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Université Pierre et Marie Curie - Paris 6 (UPMC)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS), Spectroscopie de l'atmosphère, Service de Chimie Quantique et Photophysique, Université libre de Bruxelles (ULB), National Center for Atmospheric Research [Boulder] (NCAR), and Cardon, Catherine
- Subjects
[PHYS.PHYS.PHYS-AO-PH]Physics [physics]/Physics [physics]/Atmospheric and Oceanic Physics [physics.ao-ph] ,[PHYS.PHYS.PHYS-AO-PH] Physics [physics]/Physics [physics]/Atmospheric and Oceanic Physics [physics.ao-ph] - Abstract
International audience; IASI has been monitoring the atmospheric composition for more than ten years onboard the MetOp-A and MetOp-B satellites. Over China, top-down measurements of carbon monoxide (CO), ozone (O₃), sulfur dioxide (SO₂), ammonia (NH₃) and formic acid (HCOOH) concentrations is now possible using the IASI mission. Some of these products are already distributed operationally by Eumetsat (O3MSAF framework), and others will follow soon.From the atmospheric spectra recorded by the instrument, enhanced levels of pollutants can be detected and followed over China. This talk will present the findings for an extended time period (2008-2016), and review the IASI capability to observe local and regional pollution events, as well as seasonal variations due to the monsoon and other dynamic patterns. Progresses and current limitations to derive long term trends will also be discussed.
- Published
- 2017
13. Strong constraints on aerosol–cloud interactions from volcanic eruptions
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Malavelle, FF, Haywood, JM, Jones, A, Gettelman, A, Clarisse, L, Bauduin, S, Allan, RP, Karset, IHH, Kristjánsson, JE, Oreopoulos, L, Cho, N, Lee, D, Bellouin, N, Boucher, O, Grosvenor, DP, Carslaw, KS, Dhomse, S, Mann, GW, Schmidt, A, Coe, H, Hartley, ME, Dalvi, M, Hill, AA, Johnson, BT, Johnson, CE, Knight, JR, O’Connor, FM, Partridge, DG, Stier, P, Myhre, G, Platnick, S, Stephens, GL, Takahashi, H, and Thordarson, T
- Abstract
Aerosols have a potentially large effect on climate, particularly through their interactions with clouds, but the magnitude of this effect is highly uncertain. Large volcanic eruptions produce sulfur dioxide, which in turn produces aerosols; these eruptions thus represent a natural experiment through which to quantify aerosol–cloud interactions. Here we show that the massive 2014–2015 fissure eruption in Holuhraun, Iceland, reduced the size of liquid cloud droplets—consistent with expectations—but had no discernible effect on other cloud properties. The reduction in droplet size led to cloud brightening and global-mean radiative forcing of around −0.2 watts per square metre for September to October 2014. Changes in cloud amount or cloud liquid water path, however, were undetectable, indicating that these indirect effects, and cloud systems in general, are well buffered against aerosol changes. This result will reduce uncertainties in future climate projections, because we are now able to reject results from climate models with an excessive liquid-water-path response.
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- 2017
14. Diurnal salivary alpha-amylase and not cortisol differentiates major depressive disorder in out-patients
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Bauduin, S., primary, Van Noorden, M., additional, Van der Werff, S., additional, Van Hemert, B., additional, Van der Wee, N., additional, and Giltay, E., additional
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- 2018
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15. A flexible and robust neural network IASI-NH₃
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Massachusetts Institute of Technology. Department of Civil and Environmental Engineering, Massachusetts Institute of Technology. Department of Earth, Atmospheric, and Planetary Sciences, Heald, Colette L., Whitburn, S., Van Damme, M., Clarisse, L., Bauduin, S., Hadji-Lazaro, J., Hurtmans, D., Zondlo, M. A., Clerbaux, C., Coheur, P.-F, Massachusetts Institute of Technology. Department of Civil and Environmental Engineering, Massachusetts Institute of Technology. Department of Earth, Atmospheric, and Planetary Sciences, Heald, Colette L., Whitburn, S., Van Damme, M., Clarisse, L., Bauduin, S., Hadji-Lazaro, J., Hurtmans, D., Zondlo, M. A., Clerbaux, C., and Coheur, P.-F
- Abstract
n this paper, we describe a new flexible and robust NH₃ retrieval algorithm from measurements of the Infrared Atmospheric Sounding Interferometer (IASI). The method is based on the calculation of a spectral hyperspectral range index (HRI) and subsequent conversion to NH₃ columns via a neural network. It is an extension of the method presented in Van Damme et al. (2014a) who used lookup tables (LUT) for the radiance-concentration conversion. The new method inherits the advantages of the LUT-based method while providing several significant improvements. These include the following: (1) Complete temperature and humidity vertical profiles can be accounted for. (2) Third-party NH₃ vertical profile information can be used. (3) Reported positive biases of LUT retrieval are reduced, and finally (4) a full measurement uncertainty characterization is provided. A running theme in this study, related to item (2), is the importance of the assumed vertical NH₃ profile. We demonstrate the advantages of allowing variable profile shapes in the retrieval. As an example, we analyze how the retrievals change when all NH₃ is assumed to be confined to the boundary layer. We analyze different averaging procedures in use for NH₃ in the literature, introduced to cope with the variable measurement sensitivity and derive global averaged distributions for the year 2013. A comparison with a GEOS-Chem modeled global distribution is also presented, showing a general good correspondence (within ±3 × 10¹⁵ molecules.cm⁻²) over most of the Northern Hemisphere. However, IASI finds mean columns about 1–1.5 × 10¹⁶ molecules.cm⁻² (∼50–60%) lower than GEOS-Chem for India and the North China plain., United States. National Oceanic and Atmospheric Administration (NA12OAR4310064)
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- 2017
16. First simultaneous space measurements of atmospheric pollutants in the boundary layer from IASI: a case study in the North China Plain
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Boynard, Anne, Clerbaux, Cathy, Safieddine, Sarah, Pommier, Matthieu, Hadji-Lazaro, Juliette, Oudot, Charlotte, Clarisse, L., Bauduin, S., Van Damme, M., Hutmans, D., Coheur, Pierre-François, TROPO - LATMOS, Laboratoire Atmosphères, Milieux, Observations Spatiales (LATMOS), Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Université Pierre et Marie Curie - Paris 6 (UPMC)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Université Pierre et Marie Curie - Paris 6 (UPMC)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS), Spectroscopie de l'atmosphère, Service de Chimie Quantique et Photophysique, Université libre de Bruxelles (ULB), Laboratoire des Sciences du Climat et de l'Environnement [Gif-sur-Yvette] (LSCE), Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ), Faculty of Earth and Life Sciences [Amsterdam] (FALW), Vrije Universiteit Amsterdam [Amsterdam] (VU), Centre National de la Recherche Scientifique (CNRS), Centre National d'Etudes Spatiales (CNES), European Space Agency (ESA), Communauté Française de Belgique (Actions de Recherche Concertées), Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS), Cardon, Catherine, Earth and Climate, and Amsterdam Global Change Institute
- Subjects
[PHYS.PHYS.PHYS-AO-PH]Physics [physics]/Physics [physics]/Atmospheric and Oceanic Physics [physics.ao-ph] ,[SDE] Environmental Sciences ,China ,Boundary layer ,IASI ,Satellite remote sensing ,[SDE]Environmental Sciences ,Winter air pollution ,[PHYS.PHYS.PHYS-AO-PH] Physics [physics]/Physics [physics]/Atmospheric and Oceanic Physics [physics.ao-ph] ,ComputingMilieux_MISCELLANEOUS - Abstract
International audience; An extremely severe and persistent smog episode occurred in January 2013 over China. The levels of air pollution have been dangerously high, reaching 40 times recommended safety levels and have affected health of millions of people. China faced one of the worst periods of air quality in recent history and drew worldwide attention. This pollution episode was caused by the combination of anthropogenic emissions and stable meteorological conditions (absence of wind and temperature inversion) that trapped pollutants in the boundary layer. To characterize this episode, we used the IASI (Infrared Atmospheric Sounding Interferometer) instrument onboard the MetOp-A platform. IASI observations show high concentrations of key trace gases such as carbon monoxide (CO), sulfur dioxide (SO2) and ammonia (NH3) along with ammonium sulfate aerosol. We show that IASI is able to detect boundary layer pollution in case of large negative thermal contrast combined with high levels of pollution. Our findings demonstrate the ability of thermal infrared instrument such as IASI to monitor boundary layer pollutants, which can support air quality evaluation and management.
- Published
- 2014
17. Global monitoring of near-surface sulfur dioxide (SO2) from IASI satellite observations: Method and first results
- Author
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Bauduin, S., Clarisse, L., Hurtmans, D., Clerbaux, Cathy, Coheur, Pierre-François, Cardon, Catherine, Spectroscopie de l'atmosphère, Service de Chimie Quantique et Photophysique, Université libre de Bruxelles (ULB), TROPO - LATMOS, Laboratoire Atmosphères, Milieux, Observations Spatiales (LATMOS), and Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Université Pierre et Marie Curie - Paris 6 (UPMC)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Université Pierre et Marie Curie - Paris 6 (UPMC)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)
- Subjects
[PHYS.PHYS.PHYS-AO-PH]Physics [physics]/Physics [physics]/Atmospheric and Oceanic Physics [physics.ao-ph] ,ComputingMilieux_MISCELLANEOUS ,[PHYS.PHYS.PHYS-AO-PH] Physics [physics]/Physics [physics]/Atmospheric and Oceanic Physics [physics.ao-ph] - Abstract
International audience
- Published
- 2014
18. A flexible and robust neural network IASI‐NH3 retrieval algorithm
- Author
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Whitburn, S., primary, Van Damme, M., additional, Clarisse, L., additional, Bauduin, S., additional, Heald, C. L., additional, Hadji‐Lazaro, J., additional, Hurtmans, D., additional, Zondlo, M. A., additional, Clerbaux, C., additional, and Coheur, P.‐F, additional
- Published
- 2016
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19. P.3.014 - Diurnal salivary alpha-amylase and not cortisol differentiates major depressive disorder in out-patients
- Author
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Bauduin, S., Van Noorden, M., Van der Werff, S., Van Hemert, B., Van der Wee, N., and Giltay, E.
- Published
- 2018
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20. Retrieval of near-surface sulfur dioxide (SO<sub>2</sub>) concentrations at a global scale using IASI satellite observations
- Author
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Bauduin, S., primary, Clarisse, L., additional, Hadji-Lazaro, J., additional, Theys, N., additional, Clerbaux, C., additional, and Coheur, P.-F., additional
- Published
- 2015
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21. Sulfur dioxide vertical column DOAS retrievals from the Ozone Monitoring Instrument: Global observations and comparison to ground-based and satellite data
- Author
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Theys, N., primary, De Smedt, I., additional, van Gent, J., additional, Danckaert, T., additional, Wang, T., additional, Hendrick, F., additional, Stavrakou, T., additional, Bauduin, S., additional, Clarisse, L., additional, Li, C., additional, Krotkov, N., additional, Yu, H., additional, Brenot, H., additional, and Van Roozendael, M., additional
- Published
- 2015
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22. A flexible and robust neural network IASI-NH3 retrieval algorithm.
- Author
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Whitburn, S., Van Damme, M., Clarisse, L., Bauduin, S., Heald, C. L., Hadji-Lazaro, J., Hurtmans, D., Zondlo, M. A., Clerbaux, C., and Coheur, P.-F
- Published
- 2016
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23. Detection of Masses in Mammography Through Redundant Expansions of Scale
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DUKE UNIV MEDICAL CENTER DURHAM NC DEPTOF RADIOLOGY, Laffont, V., Durupt, F., Birgen, M. A., Bauduin, S., Laine, A. F., DUKE UNIV MEDICAL CENTER DURHAM NC DEPTOF RADIOLOGY, Laffont, V., Durupt, F., Birgen, M. A., Bauduin, S., and Laine, A. F.
- Abstract
We show that dyadic scales may not be sufficient for the detection of masses in mammograms: a lesion may be too blurred on one scale, and then too fragmented at the next. In this paper, we report on the preliminary evidence of our study using a continuous wavelet transform in two dimensions with arbitrary positioning of a wavelet's center frequency channel tuned to the mass detection problem. Our goal is to detect masses in dense mammograms whose diameter is smaller than 1 cm. The aim is to be able to find the scale where the mass is best represented in terms of analysis., Papers from the 23rd Annual International Conference of the IEEE Engineering in Medicine and Biology Society, 25-28 OCT 2001, Istanbul, Turkey. See also ADM001351 for entire conference on cd-rom., The original document contains color images.
- Published
- 2001
24. Sensible heat flux and radiometric surface temperature over sparse Sahelian vegetation II. A model for the kB−1 parameter
- Author
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Lhomme, J.-P., primary, Troufleau, D., additional, Monteny, B., additional, Chehbouni, A., additional, and Bauduin, S., additional
- Published
- 1997
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25. New online sensor technology approaches commercial application
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Sabater, J., Kerneis, J.C., Bauduin, S., and Kiernan, P.
- Subjects
Papermaking machinery -- Control ,Optical detectors -- Usage ,Paper mills -- Quality management ,Business ,Forest products industry - Abstract
NEW ONLINE SENSOR TECHNOLOGY APPROACHES COMMERCIAL APPLICATION The most recent developments in paper machine control systems have been followed by dependable, continuos, online measurement devices and high-performance computerized control systems. [...]
- Published
- 1989
26. A Paper Sheet Contactless Linear Speed Measurement
- Author
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Bauduin, S. and Bolon, Ph.
- Abstract
Web speed and draw measurements on an industrial paper machine are generally obtained by means of rotating speeds. It is now possible to measure true linear speed, without contact by several techniques which are briefly reviewed. The principle of speed measurement by correlation of two optical signals is given. An instrument based on the autocorrelation of a single signal laser transducer is described as well as its signal processing specific unit. Results are presented, the main features of the instrument are discussed. Possible applications in the paper industry and on other materials are listed, having in mind process control.
- Published
- 1980
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27. Non Interacting Multivariable Paper Machine Headbox Control: Some Comparisons with Classical Loops
- Author
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Lebeau, B., Arrese, R., Bauduin, S., Grobet, R., and Foulard, C.
- Abstract
A non interacting multivariable papermachine headbox control is discussed and compared with some classical loops. The control design is based on quadratic optimization criterion with a discrete state variable process model. Two reference models are used in this control structure : Tracking model and Perturbation model. Integrators have not been used to remove steady state error. Different results are obtained on an experimental headbox, controlled by a process control computer.
- Published
- 1980
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28. Sensible heat flux and radiometric surface temperature over sparse Sahelian vegetation II. A model for the kB^-^1 parameter
- Author
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Lhomme, J.-P., Troufleau, D., Monteny, B., Chehbouni, A., and Bauduin, S.
- Published
- 1997
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- View/download PDF
29. Volcanic gas emissions and degassing dynamics at Ubinas and Sabancaya volcanoes; implications for the volatile budget of the central volcanic zone
- Author
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Moussallam, Y, Tamburello, G, Peters, N, Apaza, F, Schipper, CI, Curtis, A, Aiuppa, A, Masias, P, Boichu, M, Bauduin, S, Barnie, T, Bani, P, Giudice, G, and Moussallam, M
- Subjects
Trail By Fire ,Carbon dioxide ,IASI ,13. Climate action ,Sabancaya ,Ubinas ,DOAS ,Volcanic degassing ,UV-camera ,Multi-GAS
30. Detection of masses in mammography through redundant expansions of scale
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Laffont, V., primary, Durupt, F., additional, Birgen, M.A., additional, Bauduin, S., additional, and Laine, A.F., additional
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31. Stress-Based Topology Optimization with Fatigue Failure Constraints
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Collet, M., primary, Bruggi, M., additional, Bauduin, S., additional, and Duysinx, P., additional
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32. Detection of masses in mammography through redundant expansions of scale.
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Laffont, V., Durupt, F., Birgen, M.A., Bauduin, S., and Laine, A.F.
- Published
- 2001
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33. Volcanic gas emissions and degassing dynamics at Ubinas and Sabancaya volcanoes; implications for the volatile budget of the central volcanic zone
- Author
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Ian Schipper, Yves Moussallam, Fredy Apaza, Talfan Barnie, Aaron Curtis, Gaetano Giudice, Marie Boichu, Giancarlo Tamburello, Nial Peters, Pablo Masias, Philipson Bani, Sophie Bauduin, Alessandro Aiuppa, Manuel Moussallam, Moussallam, Y [0000-0002-4707-8943], Moussallam, M [0000-0003-0886-5423], Apollo - University of Cambridge Repository, Moussallam, Y., Tamburello, G., Peters, N., Apaza, F., Schipper, C., Curtis, A., Aiuppa, A., Masias, P., Boichu, M., Bauduin, S., Barnie, T., Bani, P., Giudice, G., Moussallam, M., Department of Geography [Cambridge, UK], University of Cambridge [UK] (CAM), Dipartimento di Scienze della Terra e del Mare [Palermo] (DiSTeM), Università degli studi di Palermo - University of Palermo, Istituto Nazionale di Geofisica e Vulcanologia - Sezione di Bologna (INGV), Istituto Nazionale di Geofisica e Vulcanologia, Department of Geography, University of Cambridge, Observatorio Vulcanológico del INGEMMET (Dirección de Geología Ambiental y Riesgo Geológico) [Arequipa], Observatorio Vulcanológico del INGEMMET (Dirección de Geología Ambiental y Riesgo Geológico), School of Earth Sciences, Victoria University of Wellington, P.O. Box 600, Wellington, New Zealand (SCHOOL OF EARTH SCIENCES, VICTORIA UNIVERSITY OF WELLINGTON, P.O. BOX 600, WELLINGTON, NEW ZEALAND), School of Earth Sciences, Victoria University of Wellington, P.O. Box 600, Wellington, New Zealand, New Mexico Institute of Mining and Technology [New Mexico Tech] (NMT), Istituto Nazionale di Geofisica e Vulcanologia - Sezione di Palermo (INGV), Laboratoire d’Optique Atmosphérique - UMR 8518 (LOA), Institut national des sciences de l'Univers (INSU - CNRS)-Université de Lille-Centre National de la Recherche Scientifique (CNRS), Centre National de la Recherche Scientifique (CNRS), Université libre de Bruxelles (ULB), Open University (School of Physical Sciences), Laboratoire Magmas et Volcans (LMV-ENSMSE), École des Mines de Saint-Étienne (Mines Saint-Étienne MSE), Institut Mines-Télécom [Paris] (IMT)-Institut Mines-Télécom [Paris] (IMT)-SPIN-Centre National de la Recherche Scientifique (CNRS)-Laboratoire Magmas et Volcans (LMV), Institut national des sciences de l'Univers (INSU - CNRS)-Université Jean Monnet - Saint-Étienne (UJM)-Institut de Recherche pour le Développement et la société-Université Clermont Auvergne [2017-2020] (UCA [2017-2020])-Centre National de la Recherche Scientifique (CNRS)-Observatoire de Physique du Globe de Clermont-Ferrand (OPGC), Institut national des sciences de l'Univers (INSU - CNRS)-Université Clermont Auvergne [2017-2020] (UCA [2017-2020])-Centre National de la Recherche Scientifique (CNRS)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Clermont Auvergne [2017-2020] (UCA [2017-2020])-Centre National de la Recherche Scientifique (CNRS)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Jean Monnet - Saint-Étienne (UJM)-Institut de Recherche pour le Développement et la société-Université Clermont Auvergne [2017-2020] (UCA [2017-2020])-Observatoire de Physique du Globe de Clermont-Ferrand (OPGC), Institut national des sciences de l'Univers (INSU - CNRS)-Université Clermont Auvergne [2017-2020] (UCA [2017-2020])-Centre National de la Recherche Scientifique (CNRS)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Clermont Auvergne [2017-2020] (UCA [2017-2020])-Centre National de la Recherche Scientifique (CNRS), Deezer R&D, Royal Geographical Society (with the Institute of BritishGeographers) with the Land Rover Bursary, Deep Carbon Observatory DECADE Initiative, Ocean Optics, Crowcon, Air Liquide, Thermo Fisher Scientific, Cactus Outdoor, Turbo Ace, TeamBlack Sheep, Scripps Institution of Oceanography Postdoctoral Fellowship program, Research startup grant from Victoria University ofWellington, Trail by fire, ANR-15-CE04-0003,VOLCPLUME,Les panaches volcaniques: emissions, chimie/transport et impact sur l'atmosphère et le climat(2015), European Project: 305377,EC:FP7:ERC,ERC-2012-StG_20111012,BRIDGE(2012), Institut national des sciences de l'Univers (INSU - CNRS)-Université Jean Monnet [Saint-Étienne] (UJM)-Institut de Recherche pour le Développement et la société-Université Clermont Auvergne [2017-2020] (UCA [2017-2020])-Centre National de la Recherche Scientifique (CNRS)-Observatoire de Physique du Globe de Clermont-Ferrand (OPGC), Centre National de la Recherche Scientifique (CNRS)-Université Clermont Auvergne [2017-2020] (UCA [2017-2020])-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Université Clermont Auvergne [2017-2020] (UCA [2017-2020])-Institut national des sciences de l'Univers (INSU - CNRS)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Jean Monnet [Saint-Étienne] (UJM)-Institut de Recherche pour le Développement et la société-Université Clermont Auvergne [2017-2020] (UCA [2017-2020])-Observatoire de Physique du Globe de Clermont-Ferrand (OPGC), and Centre National de la Recherche Scientifique (CNRS)-Université Clermont Auvergne [2017-2020] (UCA [2017-2020])-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Université Clermont Auvergne [2017-2020] (UCA [2017-2020])-Institut national des sciences de l'Univers (INSU - CNRS)
- Subjects
IASI ,010504 meteorology & atmospheric sciences ,Sabancaya ,Earth science ,Geochemistry ,010502 geochemistry & geophysics ,01 natural sciences ,Volcanic Gases ,Atmosphere ,chemistry.chemical_compound ,Flux (metallurgy) ,Geochemistry and Petrology ,[SDU.STU.VO]Sciences of the Universe [physics]/Earth Sciences/Volcanology ,Volcanic degassing ,event ,Geophysic ,0105 earth and related environmental sciences ,[SDU.OCEAN]Sciences of the Universe [physics]/Ocean, Atmosphere ,event.disaster_type ,Trail By Fire ,geography ,geography.geographical_feature_category ,Gas emissions ,UV-camera ,Ubina ,Geophysics ,Carbon dioxide ,chemistry ,Volcano ,Ubinas ,DOAS ,13. Climate action ,Multi-GAS ,Geology ,Earth (classical element) - Abstract
Emission of volcanic gas is thought to be the dominant process by which volatiles transit from the deep earth to the atmosphere. Volcanic gas emissions, remain poorly constrained, and volcanoes of Peru are entirely absent from the current global dataset. In Peru, Sabancaya and Ubinas volcanoes are by far the largest sources of volcanic gas. Here, we report the first measurements of the compositions and fluxes of volcanic gases emitted from these volcanoes. The measurements were acquired in November 2015. We determined an average SO 2 flux of 15.3 ± 2.3 kg s − 1 (1325-ton day − 1 ) at Sabancaya and of 11.4 ± 3.9 kg s − 1 (988-ton day − 1 ) at Ubinas using scanning ultraviolet spectroscopy and dual UV camera systems. In-situ Multi-GAS analyses yield molar proportions of H 2 O, CO 2 , SO 2 , H 2 S and H 2 gases of 73, 15, 10 1.15 and 0.15 mol% at Sabancaya and of 96, 2.2, 1.2 and 0.05 mol% for H 2 O, CO 2 , SO 2 and H 2 S at Ubinas. Together, these data imply cumulative fluxes for both volcanoes of 282, 30, 27, 1.2 and 0.01 kg s − 1 of H 2 O, CO 2 , SO 2 , H 2 S and H 2 respectively. Sabancaya and Ubinas volcanoes together contribute about 60% of the total CO 2 emissions from the Central Volcanic zone, and dominate by far the total revised volatile budget of the entire Central Volcanic Zone of the Andes.
- Published
- 2017
34. Simulating the efficacy of wolf-dog hybridization management with individual-based modeling.
- Author
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Santostasi NL, Bauduin S, Grente O, Gimenez O, and Ciucci P
- Abstract
Introgressive hybridization between wolves and dogs is a conservation concern due to its potentially deleterious long-term evolutionary consequences. European legislation requires that wolf-dog hybridization be mitigated through effective management. We developed an individual-based model (IBM) to simulate the life cycle of gray wolves that incorporates aspects of wolf sociality that affect hybridization rates (e.g., the dissolution of packs after the death of one/both breeders) with the goal of informing decision-making on management of wolf-dog hybridization. We applied our model by projecting hybridization dynamics in a local wolf population under different mate choice and immigration scenarios and contrasted results of removal of admixed individuals with their sterilization and release. In several scenarios, lack of management led to complete admixture, whereas reactive management interventions effectively reduced admixture in wolf populations. Management effectiveness, however, strongly depended on mate choice and number and admixture level of individuals immigrating into the wolf population. The inclusion of anthropogenic mortality affecting parental and admixed individuals (e.g., poaching) increased the probability of pack dissolution and thus increased the probability of interbreeding with dogs or admixed individuals and boosted hybridization and introgression rates in all simulation scenarios. Recognizing the necessity of additional model refinements (appropriate parameterization, thorough sensitivity analyses, and robust model validation) to generate management recommendations applicable in real-world scenarios, we maintain confidence in our model's potential as a valuable conservation tool that can be applied to diverse situations and species facing similar threats., (© 2024 The Author(s). Conservation Biology published by Wiley Periodicals LLC on behalf of Society for Conservation Biology.)
- Published
- 2024
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35. Interplay between Proline Metabolism and ROS in the Fine Tuning of Root-Meristem Size in Arabidopsis .
- Author
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Bauduin S, Latini M, Belleggia I, Migliore M, Biancucci M, Mattioli R, Francioso A, Mosca L, Funck D, and Trovato M
- Abstract
We previously reported that proline modulates root meristem size in Arabidopsis by controlling the ratio between cell division and cell differentiation. Here, we show that proline metabolism affects the levels of superoxide anion (O
2 •- ) and hydrogen peroxide (H2 O2 ), which, in turn, modulate root meristem size and root elongation. We found that hydrogen peroxide plays a major role in proline-mediated root elongation, and its effects largely overlap those induced by proline, influencing root meristem size, root elongation, and cell cycle. Though a combination of genetic and pharmacological evidence, we showed that the short-root phenotype of the proline-deficient p5cs1 p5cs2/P5CS2 , an Arabidopsis mutant homozygous for p5cs1 and heterozygous for p5cs2 , is caused by H2 O2 accumulation and is fully rescued by an effective H2 O2 scavenger. Furthermore, by studying Arabidopsis mutants devoid of ProDH activity, we disclosed the essential role of this enzyme in the modulation of root meristem size as the main enzyme responsible for H2 O2 production during proline degradation. Proline itself, on the contrary, may not be able to directly control the levels of H2 O2 , although it seems able to enhance the enzymatic activity of catalase (CAT) and ascorbate peroxidase (APX), the two most effective scavengers of H2 O2 in plant cells. We propose a model in which proline metabolism participates in a delicate antioxidant network to balance H2 O2 formation and degradation and fine-tune root meristem size in Arabidopsis .- Published
- 2022
- Full Text
- View/download PDF
36. Potential associations between immune signaling genes, deactivated microglia, and oligodendrocytes and cortical gray matter loss in patients with long-term remitted Cushing's disease.
- Author
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Bauduin SEEC, den Rooijen ILB, Meijer M, van der Werff SJA, Keo A, Dzyubachyk O, Pereira AM, Giltay EJ, van der Wee NJA, Meijer OC, and Mahfouz A
- Subjects
- Cerebral Cortex pathology, Gray Matter pathology, Humans, Hydrocortisone metabolism, Immunity genetics, Microglia physiology, Oligodendroglia physiology, Pituitary ACTH Hypersecretion genetics, Pituitary ACTH Hypersecretion pathology, Pituitary ACTH Hypersecretion physiopathology
- Abstract
Introduction: Cushing's disease (CD) is a rare and severe endocrine disease characterized by hypercortisolemia. Previous studies have found structural brain alterations in remitted CD patients compared to healthy controls, specifically in the anterior cingulate cortex (ACC). However, potential mechanisms through which these persistent alterations may have occurred are currently unknown., Methods: Structural 3T MRI's from 25 remitted CD patients were linked with gene expression data from neurotypical donors, derived from the Allen Human Brain Atlas. Differences in gene expression between the ACC and an unaffected control cortical region were examined, followed by a Gene Ontology (GO) enrichment analysis. A cell type enrichment analysis was conducted on the differentially expressed genes, and a disease association enrichment analysis was conducted to determine possible associations between differentially expressed genes and specific diseases. Subsequently, cortisol sensitivity of these genes in existing datasets was examined., Results: The gene expression analysis identified 300 differentially expressed genes in the ACC compared to the cortical control region. GO analyses found underexpressed genes to represent immune function. The cell type specificity analysis indicated that underexpressed genes were enriched for deactivated microglia and oligodendrocytes. Neither significant associations with diseases, nor evidence of cortisol sensitivity with the differentially expressed genes were found., Discussion: Underexpressed genes in the ACC, the area vulnerable to permanent changes in remitted CD patients, were often associated with immune functioning. The specific lack of deactivated microglia and oligodendrocytes implicates protective effects of these cell types against the long-term effects of cortisol overexposure., (Copyright © 2021 The Authors. Published by Elsevier Ltd.. All rights reserved.)
- Published
- 2021
- Full Text
- View/download PDF
37. Salivary markers of stress system activation and social withdrawal in humans.
- Author
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Bauduin SEEC, Giltay EJ, van Noorden MS, van der Werff SJA, de Leeuw M, van Hemert AM, and van der Wee NJA
- Subjects
- Adult, Cross-Sectional Studies, Female, Humans, Hydrocortisone, Hypothalamo-Hypophyseal System metabolism, Male, Middle Aged, Pituitary-Adrenal System metabolism, Saliva metabolism, Stress, Psychological, Mental Disorders, Salivary alpha-Amylases metabolism, Social Isolation
- Abstract
Social withdrawal is an early and common feature of psychiatric disorders. Hypothalamic-pituitary-adrenal (HPA)-axis activation through increased salivary cortisol (sC) and sympathetic activation through increased salivary alpha-amylase (sAA) may play a role. We aimed to study whether the link between increased sC and sAA on the one hand and depression on the other hand is mediated by social withdrawal. In this cross-sectional, observational study, sC and sAA measures were measured in seven saliva samples in 843 participants (231 psychiatric patients and 612 healthy controls). Social withdrawal was assessed through the Brief Symptom Inventory (BSI)-, the Short Form 36-, and the Dutch Dimensional Assessment of Personality Pathology social withdrawal subscales, and analyzed using linear regression and mediation analyses. On average, participants were 44.0 years old (SD = 12.8; 64.1% female). Basal and diurnal sAA were unrelated to any social withdrawal scale and depression. Certain sC measures were positively associated with the BSI social withdrawal subscale (i.e., area under the curve with respect to the increase, beta = 0.082, p = 0.02; evening sC value: beta = 0.110, p = 0.003; and mean sC value: beta = 0.097; p = 0.01). We found limited support for statistical mediation by social withdrawal (measured using a composite social withdrawal score) on the relationship between evening sC and depression. Thus, although we found no support for a role of basal and diurnal sAA in social withdrawal, HPA-axis activation may partly aggravate social withdrawal in depressive disorders., (Copyright © 2020 The Authors. Published by Elsevier Ltd.. All rights reserved.)
- Published
- 2021
- Full Text
- View/download PDF
38. Integrating functional connectivity in designing networks of protected areas under climate change: A caribou case-study.
- Author
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Bauduin S, Cumming SG, St-Laurent MH, and McIntire EJB
- Subjects
- Animal Migration, Animals, Computer Simulation, Ecosystem, Mammals, Biodiversity, Climate Change, Conservation of Natural Resources methods, Reindeer
- Abstract
Land-use change and climate change are recognized as two main drivers of the current biodiversity decline. Protected areas help safeguard the landscape from additional anthropogenic disturbances and, when properly designed, can help species cope with climate change impacts. When designed to protect the regional biodiversity rather than to conserve focal species or landscape elements, protected areas need to cover a representative sample of the regional biodiversity and be functionally connected, facilitating individual movements among protected areas in a network to maximize their effectiveness. We developed a methodology to define effective protected areas to implement in a regional network using ecological representativeness and functional connectivity as criteria. We illustrated this methodology in the Gaspésie region of Québec, Canada. We simulated movements for the endangered Atlantic-Gaspésie caribou population (Rangifer tarandus caribou), using an individual-based model, to determine functional connectivity based on this large mammal. We created multiple protected areas network scenarios and evaluated their ecological representativeness and functional connectivity for the current and future conditions. We selected a subset of the most effective network scenarios and extracted the protected areas included in them. There was a tradeoff between ecological representativeness and functional connectivity for the created networks. Only a few protected areas among those available were repeatedly chosen in the most effective networks. Protected areas maximizing both ecological representativeness and functional connectivity represented suitable areas to implement in an effective protected areas network. These areas ensured that a representative sample of the regional biodiversity was covered by the network, as well as maximizing the movement over time between and inside the protected areas for the focal population., Competing Interests: The authors have declared that no competing interests exist.
- Published
- 2020
- Full Text
- View/download PDF
39. Compensatory conservation measures for an endangered caribou population under climate change.
- Author
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Bauduin S, McIntire E, St-Laurent MH, and Cumming SG
- Subjects
- Animals, Population Dynamics, Animal Distribution, Biodiversity, Climate Change, Conservation of Natural Resources, Endangered Species, Reindeer physiology
- Abstract
Future human land use and climate change may disrupt movement behaviors of terrestrial animals, thereby altering the ability of individuals to move across a landscape. Some of the expected changes result from processes whose effects will be difficult to alter, such as global climate change. We present a novel framework in which we use models to (1) identify the ecological changes from these difficult-to-alter processes, as well as (2) the potential conservation measures that are best able to compensate for these changes. We illustrated this framework with the case of an endangered caribou population in Québec, Canada. We coupled a spatially explicit individual-based movement model with a range of landscape scenarios to assess the impacts of varying degrees of climate change, and the ability of conservation actions to compensate for such impacts on caribou movement behaviors. We found that (1) climate change impacts reduced movement potential, and that (2) the complete restoration of secondary roads inside protected areas was able to fully offset this reduction, suggesting that road restoration would be an effective compensatory conservation action. By evaluating conservation actions via landscape use simulated by an individual-based model, we were able to identify compensatory conservation options for an endangered species facing climate change.
- Published
- 2018
- Full Text
- View/download PDF
40. Elevated salivary alpha-amylase levels at awakening in patients with depression.
- Author
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Bauduin SEEC, van Noorden MS, van der Werff SJA, de Leeuw M, van Hemert AM, van der Wee NJA, and Giltay EJ
- Subjects
- Adult, Affect, Anxiety metabolism, Anxiety Disorders metabolism, Biomarkers, Case-Control Studies, Cohort Studies, Depression metabolism, Female, Humans, Hydrocortisone analysis, Male, Middle Aged, Saliva chemistry, alpha-Amylases analysis, Depressive Disorder, Major metabolism, Salivary alpha-Amylases analysis
- Abstract
Background: Specific Major Depressive Disorder (MDD) biomarkers could help improve our understanding of MDD pathophysiology and aid in the refinement of current MDD criteria. While salivary cortisol (SC) can differentiate between healthy controls and patients with psychiatric disorders, salivary alpha amylase (sAA), may be a putative candidate biomarker for MDD specifically., Methods: In a naturalistic cohort of consecutive out-patients and healthy controls, sAA and SC were determined in 833 participants (97 MDD patients, 142 patients with other mood, anxiety, and/or somatoform (MAS-) disorders, and 594 healthy controls). Samples were collected at 7 different time points (at awakening, after 30, 45, and 60 min, at 10:00 p.m., at 11:00 p.m., and at awakening on day 2)., Results: The mean age of the sample was 43.8 years (SD = 12.9; 63.9% female). Concerning sAA, MDD patients had higher sAA levels upon awakening on two consecutive days (p = 0.04, p = 0.01 respectively), as well as a higher area under the curve with respect to the increase (AUCi; p = 0.04) in comparison to both controls and the other MAS-disorders group. Regarding SC, mean levels of evening SC were elevated in MDD patients (p = 0.049) in comparison to both controls and the other MAS-disorders group. SC values on day 2 after ingestion of dexamethasone were elevated in both MDD patients and the other MAS-disorders group (p = 0.04, p = 0.047 respectively)., Conclusions: sAA at awakening and not cortisol differentiates MDD from other psychiatric disorders in outpatients. This suggests that sAA may be a valuable candidate biomarker specifically for MDD., (Copyright © 2018 Elsevier Ltd. All rights reserved.)
- Published
- 2018
- Full Text
- View/download PDF
41. Erratum: Strong constraints on aerosol-cloud interactions from volcanic eruptions.
- Author
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Malavelle FF, Haywood JM, Jones A, Gettelman A, Clarisse L, Bauduin S, Allan RP, Karset IHH, Kristjánsson JE, Oreopoulos L, Cho N, Lee D, Bellouin N, Boucher O, Grosvenor DP, Carslaw KS, Dhomse S, Mann GW, Schmidt A, Coe H, Hartley ME, Dalvi M, Hill AA, Johnson BT, Johnson CE, Knight JR, O'Connor FM, Partridge DG, Stier P, Myhre G, Platnick S, Stephens GL, Takahashi H, and Thordarson T
- Abstract
This corrects the article DOI: 10.1038/nature22974.
- Published
- 2017
- Full Text
- View/download PDF
42. Strong constraints on aerosol-cloud interactions from volcanic eruptions.
- Author
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Malavelle FF, Haywood JM, Jones A, Gettelman A, Clarisse L, Bauduin S, Allan RP, Karset IHH, Kristjánsson JE, Oreopoulos L, Cho N, Lee D, Bellouin N, Boucher O, Grosvenor DP, Carslaw KS, Dhomse S, Mann GW, Schmidt A, Coe H, Hartley ME, Dalvi M, Hill AA, Johnson BT, Johnson CE, Knight JR, O'Connor FM, Partridge DG, Stier P, Myhre G, Platnick S, Stephens GL, Takahashi H, and Thordarson T
- Abstract
Aerosols have a potentially large effect on climate, particularly through their interactions with clouds, but the magnitude of this effect is highly uncertain. Large volcanic eruptions produce sulfur dioxide, which in turn produces aerosols; these eruptions thus represent a natural experiment through which to quantify aerosol-cloud interactions. Here we show that the massive 2014-2015 fissure eruption in Holuhraun, Iceland, reduced the size of liquid cloud droplets-consistent with expectations-but had no discernible effect on other cloud properties. The reduction in droplet size led to cloud brightening and global-mean radiative forcing of around -0.2 watts per square metre for September to October 2014. Changes in cloud amount or cloud liquid water path, however, were undetectable, indicating that these indirect effects, and cloud systems in general, are well buffered against aerosol changes. This result will reduce uncertainties in future climate projections, because we are now able to reject results from climate models with an excessive liquid-water-path response.
- Published
- 2017
- Full Text
- View/download PDF
43. Efficacy of a granular formulation of Bacillus sphaericus against Culex quinquefasciatus and Anopheles gambiae in West African countries.
- Author
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Skovmand O and Bauduin S
- Subjects
- Africa, Western, Animals, Anopheles, Bacillus, Culex, Insecticides, Pest Control, Biological
- Abstract
The efficacy of a sustained released granular formulation of Bacillus sphaericus strain 2362 was compared to a flowable concentrate in containers, cesspools, and water ponds. Duration of control was dependent on formulation, dosage, exposure to sun, site, recycling, and target mosquito larvae. In a series of container tests with repeated additions of fourth-instar Culex quinquefasciatus larvae exposed to 0.3 or 3.0 g/m2 when cadavers were not removed, more than 95 percent control was obtained for two and four days in containers that were exposed to the sun with sewage water treated with the flowable concentrate compared to four and seven days for those treated with the granule. In sun-exposed containers with sewage water, control persisted for two days for the flowable concentrate at both dosages and one and six days for the granule at 0.3 g/m2 and 3.0 g/m2, respectively. Compared to the above tests, more than seven weeks control was obtained with 0.3 g/m2 of the flowable concentrate in closed containers where larvae were added weekly. In closed containers without weekly addition of larvae, the control was 15 percent when larvae were added five weeks after the treatment. Spore counts at the surface and bottom of the containers with lids showed an increase in number of spores at the surface where larvae were added weekly and a rapid decline where they were not. Spore counts at the bottom showed settling in both cases, but to a much higher level where larvae were added weekly. Nearly 100 percent control of Cx, quinquefasciatus larvae was obtained for at least 16 days in cesspools in Yaoundé, Cameroon, treated with the granule at 3.0 g/m2 compared to approximately nine days for the flowable concentrate. At 0.3 g/m2, the duration of this reduction was five days for both products. Nearly 100 percent control of Anopheles gambiae was obtained in sun-exposed water ponds near the village Kotiokh, Senegal, for at least 15 days with the granule at 3.0 g/m2 compared to just five days for the flowable concentrate at the same dosage.
- Published
- 1997
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